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Home > Art, Film & Photography > Chemical Oceanography: Carbon Cycle, Salinity, Nutrient, Ocean Acidification, Anoxic Event, Dead Zone, Iron Hypothesis, Seawater, F-Ratio
Chemical Oceanography: Carbon Cycle, Salinity, Nutrient, Ocean Acidification, Anoxic Event, Dead Zone, Iron Hypothesis, Seawater, F-Ratio

Chemical Oceanography: Carbon Cycle, Salinity, Nutrient, Ocean Acidification, Anoxic Event, Dead Zone, Iron Hypothesis, Seawater, F-Ratio


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About the Book

Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Pages: 45. Chapters: Carbon cycle, Salinity, Nutrient, Ocean acidification, Anoxic event, Dead zone, Iron Hypothesis, Seawater, F-ratio, Carbonaceous biochemical oxygen demand, Marine snow, Hypoxia, Sea salt, Solubility pump, Alkalinity, Continental shelf pump, Vienna Standard Mean Ocean Water, Biogeochemistry, Biological pump, Oxygen cycle, Paleosalinity, Sea foam, Global Ocean Data Analysis Project, World Ocean Atlas, Anoxic waters, Ocean chemistry, Productivity, Oxygen minimum zone, Nutrient trading, Artificial seawater, Hawaii Ocean Time-series, Sediment trap, Water quality modelling, Colored dissolved organic matter, Total inorganic carbon, Bermuda Atlantic Time-series Study, Geotraces, Carbon cycle re-balancing, Cyclic salt, Functional group, Benthic lander, Total boron, Water mass, Bjerrum plot. Excerpt: Ocean acidification is the name given to the ongoing decrease in the pH of the Earth's oceans, caused by their uptake of anthropogenic carbon dioxide from the atmosphere. Between 1751 and 1994 surface ocean pH is estimated to have decreased from approximately 8.25 to 8.14, representing an increase of approaching 30% in "acidity" (H ion concentration) in the world's oceans. The cycle between the atmosphere and the oceanThe carbon cycle describes the fluxes of carbon dioxide () between the oceans, terrestrial biosphere, lithosphere, and the atmosphere. Human activities such as the combustion of fossil fuels and land use changes have led to a new flux of into the atmosphere. About 45% has remained in the atmosphere; most of the rest has been taken up by the oceans, with some also taken up by terrestrial plants. The carbon cycle involves both organic compounds as well as inorganic carbon compounds such as carbon dioxide and the carbonates. The inorganic compounds are particularly relevant when discussing ocean acidification for it in...


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Product Details
  • ISBN-13: 9781156419939
  • Publisher: Books LLC, Wiki Series
  • Publisher Imprint: Books LLC, Wiki Series
  • Height: 246 mm
  • No of Pages: 46
  • Spine Width: 3 mm
  • Weight: 100 gr
  • ISBN-10: 115641993X
  • Publisher Date: 29 Aug 2011
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Sub Title: Carbon Cycle, Salinity, Nutrient, Ocean Acidification, Anoxic Event, Dead Zone, Iron Hypothesis, Seawater, F-Ratio
  • Width: 189 mm


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